Contenus

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  Twenty percent of agricultural management effects on organic carbon stocks occur in subsoils – Results of ten long-term experiments

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  Rates of soil organic carbon change in cultivated and afforested sandy soils

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  Meta-analysis on carbon sequestration through Conservation Agriculture in Africa

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  Maximizing soil organic carbon stocks under cover cropping: insights from long-term agricultural experiments in North America

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  Contribution of roots to soil organic carbon: From growth to decomposition experiment

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  Photosynthetic limits on carbon sequestration in croplands

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  Multi-modelling predictions show high uncertainty of required carbon input changes to reach a 4‰ target

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  Carbon saturation deficit and litter quality drive the stabilization of litter-derived C in mineral-associated organic matter in long-term no-till soil

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  How does soil water status influence the fate of soil organic matter? A review of processes across scales

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  Is it possible to attain the same soil organic matter content in arable agricultural soils as under natural vegetation?

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  A well-established fact: rapid mineralization of organic inputs is an important factor for soil carbon sequestration

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  Roots are key to increasing the mean residence time of organic carbon entering temperate agricultural soils

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  Long-term, amplified responses of soil organic carbon to nitrogen addition worldwide

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  Stability of soil organic carbon during forest conversion is more sensitive in deep soil than in topsoil in subtropical forests